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When two plates collide with enough force, faulting occurs, breaking the crust. Faulting (Apex)
When two plates carrying continental crust collide, the continental crust is too light to subduct beneath the other plate. Instead, the plates crumple and fold, leading to the formation of mountain ranges. This process is known as continental collision.
Breaks in the Earth's crust where plates meet are called plate boundaries. These boundaries are classified into three types: divergent, convergent, and transform boundaries, depending on the motion of the plates.
When tectonic plates collide they often form volcanoes or moutains. But when they slide past each other they create earthquakes...like in Haiti or Japan.
Oceanic crust is denser than continental crust, dense enough to sink into the mantle. Continental crust is not dense enough to do this.
When two plates collide with enough force, faulting occurs, breaking the crust. Faulting (Apex)
When two plates collide with enough force, faulting occurs, breaking the crust. Faulting (Apex)
When two plates collide with enough force to break the crust, it can lead to the formation of mountain ranges through the process of crustal deformation and uplift. This collision can also create intense seismic activity, such as earthquakes, as the plates interact and adjust to the intense pressure and stress. Additionally, volcanic activity may occur where magma from the mantle is forced up to the surface.
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When two plates carrying continental crust collide, the continental crust is too light to subduct beneath the other plate. Instead, the plates crumple and fold, leading to the formation of mountain ranges. This process is known as continental collision.
When two plates carrying continental crust collide, they can form mountain ranges through a process called continental collision. The intense pressure and heat generated during the collision can result in the uplift and folding of the crust, leading to the formation of large mountain belts such as the Himalayas.
When continental plates collide, the denser oceanic crust is usually subducted beneath the less dense continental crust. This process can create subduction zones, where the oceanic crust is forced downward into the mantle. The oceanic crust may melt or be recycled back into the mantle in these subduction zones.
The breaks in the crust where plates meet are called plate boundaries. These boundaries can be divergent (moving apart), convergent (moving together), or transform (sliding past each other). Earthquakes and volcanic activity often occur at plate boundaries due to the tectonic forces at work.
This is called a convergent boundary. At convergent boundaries, two tectonic plates move toward each other, resulting in compression and deformation of the Earth's crust. This can lead to the formation of mountain ranges or deep-sea trenches.
When two plates collide, or come together, the plates will push upward, forming a mountain. If one plate is continental crust and the other is oceanic crust, the less dense crust (this being the oceanic) will actually move under the more dense crust, in a process called subduction, to form a deep-ocean trench.
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Yes, it "dives" under the continental crust and back into the mantle.